摘要
白洋厂矿区以银为主,共生、伴生铜铅锌汞,系滇西首个发现的中型独立银矿床。矿区东部断裂呈弧形弯曲,并作NNW向收敛、SE方向撒开趋势,这些弧形断裂应是一帚状构造。
In Baiyangchang orefield, Ag is the main metallogenetic element. The paragenetic elements are Cu, Pb, Zn and Hg. It is the first middle scale independent Ag deposit discovered in West Yunnan. In the east part of the orefield, the trend of arcual fault is convergent NNW-wards and divergent SE-wards. These arcual faults must be a broomlike structure.
出处
《云南地质》
2004年第3期370-377,共8页
Yunnan Geology
关键词
银多金属矿
帚状构造带
控矿作用
云龙
弧形断裂
Broomlike Structure
Ore-controlling Characteristics
Ag Multimetallic Deposit
Baiyangchang,Yunlong